Isotope (δ13C and δ18O) compositions of dolomites from the Permian evaporitic sequences of the Eastern Russian Plate: Evidence from the Syukeevo gypsum deposit

dc.contributor.author	Sungatullin R.
dc.contributor.author	Kuleshov V.
dc.contributor.author	Kadyrov R.
dc.date.accessioned	2018-09-18T20:05:47Z
dc.date.available	2018-09-18T20:05:47Z
dc.date.issued	2014
dc.identifier.issn	0024-4902
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/136457
dc.description.abstract	Carbon and oxygen isotope compositions has been studied in dolomites of the Syukeevo gypsum deposit located in the Eastern Russian Plate. Values of δ13C in the dolomites vary from 0.3 to 6.6 ‰; δ18O, from 28.0 to 36.6‰. It is shown that the dolomites were formed in the epicontinental evaporitic basin in different paleoecological settings. This led to the formation of diverse lithological types of dolomites with peculiar isotope-geochemical features. © 2014 Pleiades Publishing, Inc.
dc.relation.ispartofseries	Lithology and Mineral Resources
dc.title	Isotope (δ13C and δ18O) compositions of dolomites from the Permian evaporitic sequences of the Eastern Russian Plate: Evidence from the Syukeevo gypsum deposit
dc.type	Article
dc.relation.ispartofseries-issue	5
dc.relation.ispartofseries-volume	49
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	406
dc.source.id	SCOPUS00244902-2014-49-5-SID84906494823

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Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.